Concentrations of aerosol trace elements collected from bulk aerosol samples on the 2015 US GEOTRACES Western Arctic Transect cruise on USCGC Healy (HLY1502) from August to October 2015

Website: https://www.bco-dmo.org/dataset/725905
Data Type: Cruise Results
Version: 2
Version Date: 2020-06-03

Project
» U.S. Arctic GEOTRACES Study (GN01) (U.S. GEOTRACES Arctic)
» Collaborative Research: GEOTRACES Arctic Section: Sampling and Analysis of Atmospheric Deposition (GEOTRACES Arctic Atmospheric Deposition)

Program
» U.S. GEOTRACES (U.S. GEOTRACES)
ContributorsAffiliationRole
Buck, Clifton S.Skidaway Institute of Oceanography (SkIO)Principal Investigator
Gao, YuanRutgers UniversityCo-Principal Investigator
Landing, William M.Florida State University (FSU - EOAS)Co-Principal Investigator
Rauch, ShannonWoods Hole Oceanographic Institution (WHOI BCO-DMO)BCO-DMO Data Manager

Abstract
This dataset contains concentrations of aerosol trace elements collected from bulk aerosol samples on the 2015 US GEOTRACES Western Arctic Transect (USCG Healy GN01).


Coverage

Spatial Extent: N:89.9447 E:-174.9595 S:56.0743 W:175.7522
Temporal Extent: 2015-08-10 - 2015-10-09

Dataset Description

This dataset contains concentrations of aerosol trace elements collected from bulk aerosol samples on the 2015 US GEOTRACES Western Arctic Transect (USCG Healy GN01).


Methods & Sampling

A total of fourteen 3-4 day integrated aerosol samples were collected during the US GEOTRACES Western Arctic research cruise (hereafter known as GN01), which took place from 9th August to 12th October 2015 on the USCGC Healy (cruise HLY1502). The cruise track consisted of a northward transect from Dutch Harbor, Alaska, across the Bering Sea, through the Bering Strait and across the Makarov Basin to the North Pole, followed by a return transect across the Canada Basin and back across the Bering Sea to Dutch Harbor.

Bulk aerosol samples for multiple trace element analyses were collected using one of five Tisch Environmental high-volume (~1 m³ air min⁻¹) aerosol samplers (model 5170V-BL). For each deployment, 12 replicate 47 mm diameter Whatman 41 filters were loaded on open-face filter holders (Advantec MFS) installed on the aerosol sampler on a PVC adaptor plate (Shelley et al., 2015). Filters were acid-washed before use to reduce trace element blanks, following the procedure described by Morton et al. (2013). The samplers were deployed on the ship's flying bridge, ~23 m above sea level, to minimize the influence of sea spray on samples. Samplers were controlled by wind speed and direction, through a Campbell Scientific CR800 data-logger interfaced with an anemometer and wind vane set up in close proximity to the samplers, in order to eliminate contamination from the ship's stack exhaust. This setup was used to restrict sampling to periods when relative wind speed and direction were >0.5 m s⁻¹ and from within ±60° of the bow of the ship, respectively, for at least five continuous minutes.

Total aerosol was analyzed on a ThermoScientific Element2 high-resolution ICP-MS at Florida State University.


Data Processing Description

Data have been corrected for field and analytical blank. Reported aerosol trace element concentrations values have been normalized to the volume of air filtered during sample collection. Each sample collection period (n = 14) produced 36 replicate filters. Three of those filters were digested to produce three replicate measurements of total particulate aerosol concentration. Data from the three replicates were averaged and reported along with the standard deviation. Outliers and replicate samples that were below the field blank value were not included in the mean. Data are marked as described in the datasheet.

Problem Report: The air volume sampled for Event 6197 was too low to produce reliable measurements. All data from this event are marked with the Flag=4.

Notes on concentration averages:
This dataset reports all 3 replicate values, plus the average and standard deviation of replicates, for the following event numbers: 6149, 6236, 6347, 6444. These averages are averages of 3 independent filter sample digestions, except when values were excluded because:
(a) a value was lower than 3x standard deviation of filter blank, or
(b) a value varied from the mean of the other two replicates by more than a factor of three.

A single value/replicate is reported for the following events (thus there are "nd"s in the average and standard deviation columns): 6060, 6123, 6168, 6197, 6267, 6304, 6387, 6424, 6487, 6495.

Quality Flags: Quality flag definitions follow the SeaDataNet Scheme. More information on SeaDataNet flags is available from GEOTRACES at http://www.geotraces.org/library-88/geotraces-policies/1577-geotraces-quality-flag-policy and from SeaDataNet at https://www.seadatanet.org/Standards/Data-Quality-Control. In summary:
BDL - below detection limit,
0 - No QC performed,
1 - Good data,
2 - Probably good data,
3 - Probably bad data that is potentially correctable,
4 - Bad data,
5 - Value changed,
6 - Sample < blank,
8 - Interpolated value,
9 - Missing value.

BCO-DMO Processing Notes:
- replaced blanks (missing data) with "nd";
- modified parameter names to conform with BCO-DMO naming conventions;
- added ISO_DateTime_UTC columns;
- 03 June 2020: updated to v2 (GEOTRACES IDP DOoR-formatted version).


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Data Files

File
total_aerosol.csv
(Comma Separated Values (.csv), 5.03 KB)
MD5:a31375bc334ef48e7d9c648a60bce1cf
Primary data file for dataset ID 725905

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Related Publications

Marsay, C. M., Kadko, D., Landing, W. M., Morton, P. L., Summers, B. A., & Buck, C. S. (2018). Concentrations, provenance and flux of aerosol trace elements during US GEOTRACES Western Arctic cruise GN01. Chemical Geology. doi:10.1016/j.chemgeo.2018.06.007
Methods
Morton, P. L., Landing, W. M., Hsu, S.-C., Milne, A., Aguilar-Islas, A. M., Baker, A. R., … Zamora, L. M. (2013). Methods for the sampling and analysis of marine aerosols: results from the 2008 GEOTRACES aerosol intercalibration experiment. Limnology and Oceanography: Methods, 11(2), 62–78. doi:10.4319/lom.2013.11.62
Methods
Shelley, R. U., Morton, P. L., & Landing, W. M. (2015). Elemental ratios and enrichment factors in aerosols from the US-GEOTRACES North Atlantic transects. Deep Sea Research Part II: Topical Studies in Oceanography, 116, 262–272. doi:10.1016/j.dsr2.2014.12.005
Methods

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Parameters

ParameterDescriptionUnits
Station_ID

Station number; not applicable

unitless
Start_Date_UTC

Sampling start day (UTC); format: MM/DD/YY

unitless
Start_Time_UTC

Sampling start time (UTC); format: hh:mm

unitless
Start_ISO_DateTime_UTC

Sampling start date/time (UTC) formatted to ISO8601 standard: YYYY-MM-DDThh:mmz

unitless
End_Date_UTC

Sampling end day (UTC); format: MM/DD/YY

unitless
End_Time_UTC

Sampling end time (UTC); format: hh:mm

unitless
End_ISO_DateTime_UTC

Sampling end date/time (UTC) formatted to ISO8601 standard: YYYY-MM-DDThh:mmz

unitless
Start_Latitude

Sampling start latitude

decimal degrees North
Start_Longitude

Sampling start longitude

decimal degrees East
End_Latitude

Sampling end latitude

decimal degrees North
End_Longitude

Sampling end longitude

decimal degrees East
Event_ID

GEOTRACES event number

unitless
Sample_ID

GEOTRACES sample number

unitless
Sample_Depth

Sample depth; not applicable

meters (m)
Al_A_T_CONC_HIVOL_hhnotu

Total particulate aerosol Aluminum (Al) concentration; detection limit: 7.20 pmol/m3 (detection limit air volume = 200 m3)

picomoles per cubic meter (pmol/m3)
SD1_Al_A_T_CONC_HIVOL_hhnotu

One standard deviation of Al_A_T_CONC_HIVOL_hhnotu

picomoles per cubic meter (pmol/m3)
Flag_Al_A_T_CONC_HIVOL_hhnotu

Quality flag for Al_A_T_CONC_HIVOL_hhnotu

None
Cd_A_T_CONC_HIVOL_crirkf

Total particulate aerosol Cadmium (Cd) concentration; detection limit: 0.00014 pmol/m3 (detection limit air volume = 200 m3)

picomoles per cubic meter (pmol/m3)
SD1_Cd_A_T_CONC_HIVOL_crirkf

One standard deviation of Cd_A_T_CONC_HIVOL_crirkf

picomoles per cubic meter (pmol/m3)
Flag_Cd_A_T_CONC_HIVOL_crirkf

Quality flag for Cd_A_T_CONC_HIVOL_crirkf

None
Co_A_T_CONC_HIVOL_hz1byp

Total particulate aerosol Cobalt (Co) concentration; detection limit: 0.005 pmol/m3 (detection limit air volume = 200 m3)

picomoles per cubic meter (pmol/m3)
SD1_Co_A_T_CONC_HIVOL_hz1byp

One standard deviation of Co_A_T_CONC_HIVOL_hz1byp

picomoles per cubic meter (pmol/m3)
Flag_Co_A_T_CONC_HIVOL_hz1byp

Quality flag for Co_A_T_CONC_HIVOL_hz1byp

None
Cr_A_T_CONC_HIVOL_tgwnfu

Total particulate aerosol Chromium (Cr) concentration; detection limit: 0.217 pmol/m3 (detection limit air volume = 200 m3)

picomoles per cubic meter (pmol/m3)
SD1_Cr_A_T_CONC_HIVOL_tgwnfu

One standard deviation of Cr_A_T_CONC_HIVOL_tgwnfu

picomoles per cubic meter (pmol/m3)
Flag_Cr_A_T_CONC_HIVOL_tgwnfu

Quality flag for Cr_A_T_CONC_HIVOL_tgwnfu

None
Cu_A_T_CONC_HIVOL_vryvm8

Total particulate aerosol Copper (Cu) concentration; detection limit: 0.0058 pmol/m3 (detection limit air volume = 200 m3)

picomoles per cubic meter (pmol/m3)
SD1_Cu_A_T_CONC_HIVOL_vryvm8

One standard deviation of Cu_A_T_CONC_HIVOL_vryvm8

picomoles per cubic meter (pmol/m3)
Flag_Cu_A_T_CONC_HIVOL_vryvm8

Quality flag for Cu_A_T_CONC_HIVOL_vryvm8

None
Fe_A_T_CONC_HIVOL_j4eghp

Total particulate aerosol Iron (Fe) concentration; detection limit: 3.33 pmol/m3 (detection limit air volume = 200 m3)

picomoles per cubic meter (pmol/m3)
SD1_Fe_A_T_CONC_HIVOL_j4eghp

One standard deviation of Fe_A_T_CONC_HIVOL_j4eghp

picomoles per cubic meter (pmol/m3)
Flag_Fe_A_T_CONC_HIVOL_j4eghp

Quality flag for Fe_A_T_CONC_HIVOL_j4eghp

None
Mn_A_T_CONC_HIVOL_4917sh

Total particulate aerosol Manganese (Mn) concentration; detection limit: 0.025 pmol/m3 (detection limit air volume = 200 m3)

picomoles per cubic meter (pmol/m3)
SD1_Mn_A_T_CONC_HIVOL_4917sh

One standard deviation of Mn_A_T_CONC_HIVOL_4917sh

picomoles per cubic meter (pmol/m3)
Flag_Mn_A_T_CONC_HIVOL_4917sh

Quality flag for Mn_A_T_CONC_HIVOL_4917sh

None
Ni_A_T_CONC_HIVOL_uyzywk

Total particulate aerosol Nickel (Ni) concentration; detection limit: 0.557 pmol/m3 (detection limit air volume = 200 m3)

picomoles per cubic meter (pmol/m3)
SD1_Ni_A_T_CONC_HIVOL_uyzywk

One standard deviation of Ni_A_T_CONC_HIVOL_uyzywk

picomoles per cubic meter (pmol/m3)
Flag_Ni_A_T_CONC_HIVOL_uyzywk

Quality flag for Ni_A_T_CONC_HIVOL_uyzywk

None
P_A_T_CONC_HIVOL_o8q5bp

Total particulate aerosol Phosphorus (P) concentration; detection limit: 6.20 pmol/m3 (detection limit air volume = 200 m3)

picomoles per cubic meter (pmol/m3)
SD1_P_A_T_CONC_HIVOL_o8q5bp

One standard deviation of P_A_T_CONC_HIVOL_o8q5bp

picomoles per cubic meter (pmol/m3)
Flag_P_A_T_CONC_HIVOL_o8q5bp

Quality flag for P_A_T_CONC_HIVOL_o8q5bp

None
Pb_A_T_CONC_HIVOL_bh8k9t

Total particulate aerosol Lead (Pb) concentration; detection limit: 0.00098 pmol/m3 (detection limit air volume = 200 m3)

picomoles per cubic meter (pmol/m3)
SD1_Pb_A_T_CONC_HIVOL_bh8k9t

One standard deviation of Pb_A_T_CONC_HIVOL_bh8k9t

picomoles per cubic meter (pmol/m3)
Flag_Pb_A_T_CONC_HIVOL_bh8k9t

Quality flag for Pb_A_T_CONC_HIVOL_bh8k9t

None
Ti_A_T_CONC_HIVOL_29sg3r

Total particulate aerosol Titanium (Ti) concentration; detection limit: 1.047 pmol/m3 (detection limit air volume = 200 m3)

picomoles per cubic meter (pmol/m3)
SD1_Ti_A_T_CONC_HIVOL_29sg3r

One standard deviation of Ti_A_T_CONC_HIVOL_29sg3r

picomoles per cubic meter (pmol/m3)
Flag_Ti_A_T_CONC_HIVOL_29sg3r

Quality flag for Ti_A_T_CONC_HIVOL_29sg3r

None
V_A_T_CONC_HIVOL_kqq9rk

Total particulate aerosol Vanadium (V) concentration; detection limit: 0.0081 pmol/m3 (detection limit air volume = 200 m3)

picomoles per cubic meter (pmol/m3)
SD1_V_A_T_CONC_HIVOL_kqq9rk

One standard deviation of V_A_T_CONC_HIVOL_kqq9rk

picomoles per cubic meter (pmol/m3)
Flag_V_A_T_CONC_HIVOL_kqq9rk

Quality flag for V_A_T_CONC_HIVOL_kqq9rk

None
Zn_A_T_CONC_HIVOL_wtmnlj

Total particulate aerosol Zinc (Zn) concentration; detection limit: 0.254 pmol/m3 (detection limit air volume = 200 m3)

picomoles per cubic meter (pmol/m3)
SD1_Zn_A_T_CONC_HIVOL_wtmnlj

One standard deviation of Zn_A_T_CONC_HIVOL_wtmnlj

picomoles per cubic meter (pmol/m3)
Flag_Zn_A_T_CONC_HIVOL_wtmnlj

Quality flag for Zn_A_T_CONC_HIVOL_wtmnlj

None


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Instruments

Dataset-specific Instrument Name
Tisch Environmental high-volume aerosol samplers
Generic Instrument Name
Aerosol Sampler
Dataset-specific Description
Tisch Environmental high-volume (~1 m3 air min-1) aerosol samplers (model 5170V-BL) were used for sample collection.
Generic Instrument Description
A device that collects a sample of aerosol (dry particles or liquid droplets) from the atmosphere.

Dataset-specific Instrument Name
ThermoScientific Element2 high-resolution ICP-MS
Generic Instrument Name
Inductively Coupled Plasma Mass Spectrometer
Dataset-specific Description
Total aerosol was analyzed on a ThermoScientific Element2 high-resolution ICP-MS at Florida State University.
Generic Instrument Description
An ICP Mass Spec is an instrument that passes nebulized samples into an inductively-coupled gas plasma (8-10000 K) where they are atomized and ionized. Ions of specific mass-to-charge ratios are quantified in a quadrupole mass spectrometer.


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Deployments

HLY1502

Website
Platform
USCGC Healy
Report
Start Date
2015-08-09
End Date
2015-10-12
Description
Arctic transect encompassing Bering and Chukchi Shelves and the Canadian, Makarov and Amundsen sub-basins of the Arctic Ocean. The transect started in the Bering Sea (60°N) and traveled northward across the Bering Shelf, through the Bering Strait and across the Chukchi shelf, then traversing along 170-180°W across the Alpha-Mendeleev and Lomonosov Ridges to the North Pole (Amundsen basin, 90°N), and then back southward along ~150°W to terminate on the Chukchi Shelf (72°N). Additional cruise information is available in the GO-SHIP Cruise Report (PDF) and from the Rolling Deck to Repository (R2R): https://www.rvdata.us/search/cruise/HLY1502


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Project Information

U.S. Arctic GEOTRACES Study (GN01) (U.S. GEOTRACES Arctic)


Coverage: Arctic Ocean; Sailing from Dutch Harbor to Dutch Harbor (GN01)


Description from NSF award abstract:
In pursuit of its goal "to identify processes and quantify fluxes that control the distributions of key trace elements and isotopes in the ocean, and to establish the sensitivity of these distributions to changing environmental conditions", in 2015 the International GEOTRACES Program will embark on several years of research in the Arctic Ocean. In a region where climate warming and general environmental change are occurring at amazing speed, research such as this is important for understanding the current state of Arctic Ocean geochemistry and for developing predictive capability as the regional ecosystem continues to warm and influence global oceanic and climatic conditions. The three investigators funded on this award, will manage a large team of U.S.scientists who will compete through the regular NSF proposal process to contribute their own unique expertise in marine trace metal, isotopic, and carbon cycle geochemistry to the U.S. effort. The three managers will be responsible for arranging and overseeing at-sea technical services such as hydrographic measurements, nutrient analyses, and around-the-clock management of on-deck sampling activites upon which all participants depend, and for organizing all pre- and post-cruise technical support and scientific meetings. The management team will also lead educational outreach activities for the general public in Nome and Barrow, Alaska, to explain the significance of the study to these communities and to learn from residents' insights on observed changes in the marine system. The project itself will provide for the support and training of a number of pre-doctoral students and post-doctoral researchers. Inasmuch as the Arctic Ocean is an epicenter of global climate change, findings of this study are expected to advance present capability to forecast changes in regional and globlal ecosystem and climate system functioning.

As the United States' contribution to the International GEOTRACES Arctic Ocean initiative, this project will be part of an ongoing multi-national effort to further scientific knowledge about trace elements and isotopes in the world ocean. This U.S. expedition will focus on the western Arctic Ocean in the boreal summer of 2015. The scientific team will consist of the management team funded through this award plus a team of scientists from U.S. academic institutions who will have successfully competed for and received NSF funds for specific science projects in time to participate in the final stages of cruise planning. The cruise track segments will include the Bering Strait, Chukchi shelf, and the deep Canada Basin. Several stations will be designated as so-called super stations for intense study of atmospheric aerosols, sea ice, and sediment chemistry as well as water-column processes. In total, the set of coordinated international expeditions will involve the deployment of ice-capable research ships from 6 nations (US, Canada, Germany, Sweden, UK, and Russia) across different parts of the Arctic Ocean, and application of state-of-the-art methods to unravel the complex dynamics of trace metals and isotopes that are important as oceanographic and biogeochemical tracers in the sea.


Collaborative Research: GEOTRACES Arctic Section: Sampling and Analysis of Atmospheric Deposition (GEOTRACES Arctic Atmospheric Deposition)


NSF Award Abstract:
In this project, a group of investigators participating in the 2015 U.S. GEOTRACES Arctic Ocean expedition will study the distribution of a variety of trace elements in seawater, sea ice, and marine air. It is important to understand where they are and how they move in the Arctic because some trace elements are essential to life, others are known biological toxins, and still others are important because they can be used as tracers of a variety of physical, chemical, and biological processes in the sea. In common with other multinational initiatives in the International GEOTRACES Program, the goals of the U.S. Arctic expedition are to identify processes and quantify fluxes that control the distributions of key trace elements and isotopes in the ocean, and to establish the sensitivity of these distributions to changing environmental conditions. This multi-institutional team of ocean trace element experts will focus its attention on the importance of aerosol, precipitation, and sea ice melt water in trace element cycling. Results from this work will be disseminated through public educational initiatives, such as web communications and outreach to members of the public, including indigenous populations in Alaska. The project will also provide training for graduate and undergraduate students in biology and chemistry.

Atmospheric deposition is an important pathway and transport mechanism of both natural aerosols and contaminants to the ocean. Relative to other regions, atmospheric deposition rates in the Arctic are low and aerosols and dissolved chemicals in precipitation may be deposited directly to the sea surface or, unique to polar regions, onto sea ice. Given the unique biogeochemical processes of the region and its rapid changes in response to global climate change, quantifying the current atmospheric deposition of trace elements and isotopes to differing catchments (ocean, sea ice, and melt ponds) in the Arctic is critical to our ability to predict how their distribution may evolve over time. In this study, aerosol, precipitation, and melt water samples will be collected and analyzed for trace elements and isotopes in order to evaluate the impacts on the surface ocean and sea ice chemistry from natural and anthropogenic aerosols. Through this project, collected atmospheric samples from the Arctic will also be made available for distribution to the broader scientific community.



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Program Information

U.S. GEOTRACES (U.S. GEOTRACES)


Coverage: Global


GEOTRACES is a SCOR sponsored program; and funding for program infrastructure development is provided by the U.S. National Science Foundation.

GEOTRACES gained momentum following a special symposium, S02: Biogeochemical cycling of trace elements and isotopes in the ocean and applications to constrain contemporary marine processes (GEOSECS II), at a 2003 Goldschmidt meeting convened in Japan. The GEOSECS II acronym referred to the Geochemical Ocean Section Studies To determine full water column distributions of selected trace elements and isotopes, including their concentration, chemical speciation, and physical form, along a sufficient number of sections in each ocean basin to establish the principal relationships between these distributions and with more traditional hydrographic parameters;

* To evaluate the sources, sinks, and internal cycling of these species and thereby characterize more completely the physical, chemical and biological processes regulating their distributions, and the sensitivity of these processes to global change; and

* To understand the processes that control the concentrations of geochemical species used for proxies of the past environment, both in the water column and in the substrates that reflect the water column.

GEOTRACES will be global in scope, consisting of ocean sections complemented by regional process studies. Sections and process studies will combine fieldwork, laboratory experiments and modelling. Beyond realizing the scientific objectives identified above, a natural outcome of this work will be to build a community of marine scientists who understand the processes regulating trace element cycles sufficiently well to exploit this knowledge reliably in future interdisciplinary studies.

Expand "Projects" below for information about and data resulting from individual US GEOTRACES research projects.



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Funding

Funding SourceAward
NSF Division of Ocean Sciences (NSF OCE)
NSF Division of Ocean Sciences (NSF OCE)
NSF Division of Ocean Sciences (NSF OCE)

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